Linked from

The 12 pages that link to Argon–argon dating, each with the reason it gives.

• Radiometric datingBroader topic: It refines potassium–argon dating and can reveal whether a sample records multiple heating events.

• GeochronologyBroader topic: It can date small volcanic samples and test whether heating disturbed their history.

• Potassium-40Broader topic: It derives ages from potassium-40 decay while allowing multiple measurements on one mineral sample.

• Central Atlantic Magmatic ProvinceRelated: It has helped establish the timing of CAMP lava flows and intrusions.

• Rubidium–strontium datingCompared with: It often targets cooling ages in minerals where rubidium–strontium systems may record different events.

• ThermochronologyBroader topic: Argon loss during heating lets some applications constrain cooling through higher-temperature ranges.

• Alkali feldsparRelated: Potassium-bearing feldspar can record argon-loss histories used in this method.

• Closure temperatureRelated: Argon retention during cooling gives this method sensitivity to mineral thermal histories.

• Isochron datingCompared with: It uses irradiation and step-heating measurements rather than a line across co-genetic materials.

• AluniteRelated: Potassium-bearing alunite can preserve ages of hydrothermal alteration.

• Monazite geochronologyCompared with: Unlike monazite dating, it commonly tracks cooling through argon-retention temperatures.

• K–Ar datingCompared with: It derives potassium information from argon measurements and often permits analysis of smaller samples.